As with acid–base and complexation titrations, redox titrations are not frequently used in modern analytical laboratories. Nevertheless, several important applications continue to find favor in environmental, pharmaceutical, and industrial laborato- ries. In this section we review the general application of redox titrimetry. We begin, however, with a brief discussion of selecting and characterizing redox titrants, and methods for controlling the analyte’s oxidation state.
If a redox titration is to be used in a quantitative analysis, the analyte must initially be present in a single oxidation state. For example, the iron content of a sample can be determined by a redox titration in which Ce4+ oxidizes Fe2+ to Fe3+. The process of preparing the sample for analysis must ensure that all iron is present as Fe2+. Depending on the sample and the method of sample preparation, however, the iron may initially be present in both the +2 and +3 oxidation states. Before titrating, any Fe3+ that is present must be re- duced to Fe2+. This type of pretreatment can be accomplished with an auxiliary re- ducing or oxidizing agent.
Metals that are easily oxidized, such as Zn, Al, and Ag, can serve as auxiliary re- ducing agents. The metal, as a coiled wire or powder, is placed directly in the solu- tion where it reduces the analyte. Of course any unreacted auxiliary reducing agent will interfere with the analysis by reacting with the titrant. The residual auxiliary re- ducing agent, therefore, must be removed once the analyte is completely reduced. This can be accomplished by simply removing the coiled wire or by filtering.
An alternative approach to using an auxiliary reducing agent is to immobilize it in a column. To prepare a reduction column, an aqueous slurry of the finely divided metal is packed in a glass tube equipped with a porous plug at the bottom (Figure 9.39). The sample is placed at the top of the column and moves through the column under the influence of gravity or vacuum suction. The length of the reduction col- umn and the flow rate are selected to ensure the analyte’s complete reduction.
Two common reduction columns are used. In the Jones reductor the column is filled with amalgamated Zn prepared by briefly placing Zn granules in a solution of HgCl2 to form Zn(Hg). Oxidation of the amalgamated Zn
Zn(Hg)(s) < = = = = > Zn2+(aq) + Hg(l)+ 2e–
provides the electrons for reducing the analyte. In the Walden reductor the column is filled with granular Ag metal. The solution containing the analyte is acidified with HCl and passed through the column where the oxidation of Ag
Ag(s)+ Cl–(aq)< == == > AgCl(s)+ e–
provides the necessary electrons for reducing the analyte. Examples of both reduc- tion columns are shown in Table 9.19.
Several reagents are commonly used as auxiliary oxidizing agents, including ammonium peroxydisulfate, (NH4)2S2O8, and hydrogen peroxide, H2O2. Ammo- nium peroxydisulfate is a powerful oxidizing agent
S2O 2–(aq)+ 2e– < == == > 2SO42–(aq)
H2O2(aq)+ 2H3O+(aq)+ 2e– < = = = = > 4H2O(l)
provides another method for oxidizing an analyte. Excess H2O2 also can be de- stroyed by briefly boiling the solution.
In quantitative work the titrant’s concen- tration must remain stable during the analysis. Since titrants in a reduced state are susceptible to air oxidation, most redox titrations are carried out using an oxidizing agent as the titrant. The choice of which of several common oxidizing titrants is best for a particular analysis depends on the ease with which the analyte can be oxidized. Analytes that are strong reducing agents can be successfully titrated with a relatively weak oxidizing titrant, whereas a strong oxidizing titrant is required for the analysis of analytes that are weak reducing agents.
The two strongest oxidizing titrants are MnO4– and Ce4+, for which the reduc- tion half-reactions are
MnO4–(aq)+ 8H3O+(aq)+ 5e– t< = = = > Mn2+(aq) + 12H2O(l)
Ce4+(aq)+ e– < == == > Ce3+(aq)
Solutions of MnO4– are prepared from KMnO4, which is not available as a pri- mary standard. Aqueous solutions of permanganate are thermodynamically unsta- ble due to its ability to oxidize water.
4MnO4–(aq)+ 2H2O(l) < == == > 4MnO2(s)+ 3O2(g) + 4OH–(aq)
This reaction is catalyzed by the presence of MnO2, Mn2+, heat, light, and the pres- ence of acids and bases. Moderately stable solutions of permanganate can be pre- pared by boiling for an hour and filtering through a sintered glass filter to remove any solid MnO2 that precipitates. Solutions prepared in this fashion are stable for 1–2 weeks, although the standardization should be rechecked periodically. Stan- dardization may be accomplished using the same primary standard reducing agents that are used with Ce4+, using the pink color of MnO4– to signal the end point (Table 9.20).
Potassium dichromate is a relatively strong oxidizing agent whose principal ad- vantages are its availability as a primary standard and the long-term stability of its solutions. It is not, however, as strong an oxidizing agent as MnO4– or Ce4+, which prevents its application to the analysis of analytes that are weak reducing agents. Its reduction half-reaction is
Cr2O72–(aq) + 14H3O+(aq)+ 6e– < = = = = > 2Cr3+(aq) + 21H2O(l)
Although solutions of Cr2O72– are orange and those of Cr3+ are green, neither color is intense enough to serve as a useful indicator. Diphenylamine sulfonic acid, whose oxidized form is purple and reduced form is colorless, gives a very distinct end point signal with Cr2O72–.
Iodine is another commonly encountered oxidizing titrant. In comparison with MnO4–, Ce4+, and Cr2O72–, it is a weak oxidizing agent and is useful only for the analysis of analytes that are strong reducing agents. This apparent limitation, how- ever, makes I2 a more selective titrant for the analysis of a strong reducing agent in the presence of weaker reducing agents. The reduction half-reaction for I2 is
I2(aq)+ 2e– < = = = = > 2I–(aq)
Because of iodine’s poor solubility, solutions are prepared by adding an excess of I–. The complexation reaction
I2(aq)+ I–(aq) < = = = = > I3–(aq)
increases the solubility of I2 by forming the more soluble triiodide ion, I3–. Even though iodine is present as I3– instead of I2, the number of electrons in the reduc- tion half-reaction is unaffected.
I3–(aq)+ 2e– < = = = = > 3I–(aq)
Solutions of I3– are normally standardized against Na2S2O3 (see Table 9.20) using starch as a specific indicator for I3–.
Oxidizing titrants such as MnO4–, Ce4+, Cr2O72– and I3–, are used to titrate ana- lytes that are in a reduced state. When the analyte is in an oxidized state, it can be reduced with an auxiliary reducing agent and titrated with an oxidizing titrant. Al- ternatively, the analyte can be titrated with a suitable reducing titrant. Iodide is a relatively strong reducing agent that potentially could be used for the analysis of an- alytes in higher oxidation states. Unfortunately, solutions of I– cannot be used as a direct titrant because they are subject to the air oxidation of I– to I3–.
3I–(aq) < = = = = > I3–(aq)+ 2e–
Instead, an excess of KI is added, reducing the analyte and liberating a stoichiometric amount of I3–. The amount of I3– produced is then determined by a back titra- tion using Na2S2O3 as a reducing titrant.
2S2O 2–(aq) < = = = = > S4O 2–(aq)+ 2e–
IO3–(aq)+ 8I–(aq)+ 6H3O+(aq) < == = > 3I3–(aq)+ 9H O(l)
Redox titrimetry has been used for the analysis of a wide range of inorganic analytes. Although many of these methods have been replaced by newer methods, a few continue to be listed as standard methods of analysis. In this section we consider the application of redox titrimetry to several important envi- ronmental, public health, and industrial analyses.
One of the most important applications of redox titrimetry is in evaluating the chlorination of public water supplies. In Method 9.3 an approach for determining the total chlorine residual was described in which the oxidizing power of chlorine is used to oxidize I– to I3–. The amount of I3– formed is determined by a back titration with S2O32–.
The efficiency of chlorination depends on the form of the chlorinating species. For this reason it is important to distinguish between the free chlorine residual, due to Cl2, HOCl, and OCl–, and the combined chlorine residual. The latter form of chlorine results from the reaction of ammonia with the free chlo- rine residual, forming NH2Cl, NHCl2, and NCl3. When a sample of iodide-free chlorinated water is mixed with an excess of the indicator N,N-diethyl-p- phenylenediamine (DPD), the free chlorine oxidizes a stoichiometric portion of DPD to its red-colored form. The oxidized DPD is then titrated back to its color- less form with ferrous ammonium sulfate, with the volume of titrant being pro- portional to the amount of free residual chlorine. Adding a small amount of KI reduces monochloramine, NH2Cl, forming I3–. The I3– then oxidizes a portion of the DPD to its red-colored form. Titrating the oxidized DPD with ferrous am- monium sulfate yields the amount of NH2Cl in the sample. The amount of dichloramine and trichloramine are determined in a similar fashion.
The methods described earlier for determining the total, free, or combined chlorine residual also are used in establishing the chlorine demand of a water sup- ply. The chlorine demand is defined as the quantity of chlorine that must be added to a water supply to completely react with any substance that can be oxi- dized by chlorine while also maintaining the desired chlorine residual. It is deter- mined by adding progressively greater amounts of chlorine to a set of samples drawn from the water supply and determining the total, free, or combined chlo- rine residual.
Another important example of redox titrimetry that finds applications in both public health and environmental analyses is the determination of dissolved oxygen. In natural waters the level of dissolved O2 is important for two reasons: it is the most readily available oxidant for the biological oxidation of inorganic and organic pollutants; and it is necessary for the support of aquatic life. In wastewater treat- ment plants, the control of dissolved O2 is essential for the aerobic oxidation of waste materials. If the level of dissolved O2 falls below a critical value, aerobic bacte- ria are replaced by anaerobic bacteria, and the oxidation of organic waste produces undesirable gases such as CH4 and H2S.
One standard method for determining the dissolved O2 content of natural wa- ters and wastewaters is the Winkler method. A sample of water is collected in a fash- ion that prevents its exposure to the atmosphere (which might change the level of dissolved O2). The sample is then treated with a solution of MnSO4, and then with a solution of NaOH and KI. Under these alkaline conditions Mn2+ is oxidized to MnO2 by the dissolved oxygen.
2Mn2+(aq) + 4OH–(aq)+ O2(aq) → 2MnO2(s)+ 2H2O(l)
After the reaction is complete, the solution is acidified with H2SO4. Under the now acidic conditions I– is oxidized to I3– by MnO2.
The amount of I3– formed is determined by titrating with S2O32– using starch as an indicator. The Winkler method is subject to a variety of interferences, and several modifications to the original procedure have been proposed. For example, NO2– in- terferes because it can reduce I3– to I– under acidic conditions. This interference is eliminated by adding sodium azide, NaN3, reducing NO2– to N2. Other reducing agents, such as Fe2+, are eliminated by pretreating the sample with KMnO4, and de- stroying the excess permanganate with K2C2O4.
py . I2 + py . SO2 + py+ H2O → 2py . HI+ py . SO3
Methanol is included to prevent the further reaction of py . SO3 with water. The titration’s end point is signaled when the solution changes from the yellow color of the products to the brown color of the Karl Fischer reagent.
Redox titrimetric methods also are used for the analysis of or- ganic analytes. One important example is the determination of the chemical oxygen demand (COD) in natural waters and wastewaters. The COD provides a measure of the quantity of oxygen necessary to completely oxidize all the organic matter in a sample to CO2 and H2O. No attempt is made to correct for organic matter that can- not be decomposed biologically or for which the decomposition kinetics are very slow. Thus, the COD always overestimates a sample’s true oxygen demand. The de- termination of COD is particularly important in managing industrial wastewater treatment facilities where it is used to monitor the release of organic-rich wastes into municipal sewer systems or the environment.
The COD is determined by refluxing the sample in the presence of excess K2Cr2O7, which serves as the oxidizing agent. The solution is acidified with H2SO4, and Ag2SO4 is added as a catalyst to speed the oxidation of low-molecular-weight fatty acids. Mercuric sulfate, HgSO4, is added to complex any chloride that is pres- ent, thus preventing the precipitation of the Ag+ catalyst as AgCl. Under these con- ditions, the efficiency for oxidizing organic matter is 95–100%. After refluxing for 2h, the solution is cooled to room temperature, and the excess Cr2O72– is deter- mined by a back titration, using ferrous ammonium sulfate as the titrant and fer- roin as the indicator. Since it is difficult to completely remove all traces of organic matter from the reagents, a blank titration must be performed. The difference in the amount of ferrous ammonium sulfate needed to titrate the blank and the sample is proportional to the COD.
Iodine has been used as an oxidizing titrant for a number of compounds of pharmaceutical interest. Earlier we noted that the reaction of S2O32– with I3– pro- duces the tetrathionate ion, S4O62–. The tetrathionate ion is actually a dimer consist- ing of two thiosulfate ions connected through a disulfide (-S-S-) linkage. In the same fashion, I3– can be used to titrate mercaptans of the general formula RSH, forming the dimer RSSR as a product. The amino acid cysteine also can be titrated with I3–. The product of this titration is cystine, which is a dimer of cysteine. Triio- dide also can be used for the analysis of ascorbic acid (vitamin C) by oxidizing the enediol functional group to an alpha diketone
and for the analysis of reducing sugars, such as glucose, by oxidizing the aldehyde functional group to a carboxylate ion in a basic solution.
Organic compounds containing a hydroxyl, carbonyl, or amine functional group adjacent to a hydoxyl or carbonyl group can be oxidized using metaperio- date, IO3–, as an oxidizing titrant.
IO3–(aq)+H O(l)+ 2e– → IO3–(aq) + 2OH–(aq)
The analysis is conducted by adding a known excess of IO3– to the solution contain- ing the analyte and allowing the oxidation to take place for approximately 1 h at room temperature. When the oxidation is complete, an excess of KI is added, which reacts with the unreacted IO3– to form IO3– and I3–.
IO3–(aq)+ 3I–(aq)+H O(l) → IO3–(aq)+I3–(aq) + 2OH–(aq)
he I3– is then determined by titrating with S2O32– using starch as an indicator.
The stoichiometry of a redox reaction is given by the con- servation of electrons between the oxidizing and reducing agents; thus
Example 9.13 shows how this equation is applied to an analysis based on a direct titration.
Copyright © 2018-2021 BrainKart.com; All Rights Reserved. (BS) Developed by Therithal info, Chennai.